Mobilization of old terrestrial carbon caused by permafrost thawing, sea-level rise and ice-sheet melting during the last deglaciation
The last deglaciation was characterized by rising concentrations in atmospheric CO2 (CO2atm) and a decrease in its radiocarbon content (∆14Catm). Mobilization of 14C-depleted terrestrial organic carbon, which was previously frozen in extensive boreal permafrost soils, might have contributed to both...
Main Authors: | , , , , , , , , , , , , |
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Format: | Conference Object |
Language: | unknown |
Published: |
2018
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Subjects: | |
Online Access: | https://epic.awi.de/id/eprint/47461/ https://hdl.handle.net/10013/epic.4bd16db3-994e-4b37-8bfd-838adad294eb |